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. 2022 Jul 22;12:12537. doi: 10.1038/s41598-022-16693-3

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© The Author(s) 2022

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

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(a) Stratigraphy in the region studied. Pink, orange, blue, magenta, and gray represent crystalline, sandstone, limestone, evaporites, and shale rocks¹². (b) Stratigraphy based on data from a coring well (purple well in Fig. 2). (c) Cross-section of the 3D seismic survey showing the interpreted Precambrian basement. (d) Synthetic seismogram tie of a key well. (e) Original seismic profile from 3D seismic survey. (f) Trace amplitude grain control. (g) Structural smoothing. (h) Variance (edge method). (i) Ant tracking inversion³⁰.